A characteristic of a 'nimbus' cloud is its ability to produce precipitation. These clouds are typically thick and dark, indicating the presence of water droplets or ice crystals that are heavy enough to fall as rain or snow. Nimbus clouds are often associated with stormy weather, as they can bring heavy rain, thunderstorms, and even severe weather events such as hail or tornadoes.

One of the most common types of nimbus clouds is the nimbostratus cloud. These clouds form a thick, gray layer that can cover the sky for long periods of time, bringing steady, moderate rainfall. Nimbostratus clouds are often seen on overcast days when the weather is gloomy and damp.

Another type of nimbus cloud is the cumulonimbus cloud, which is known for its towering height and anvil-like shape. Cumulonimbus clouds can produce intense thunderstorms, with heavy rain, lightning, and strong winds. These clouds can also produce hail and tornadoes, making them some of the most dangerous and powerful storm clouds.

Nimbus clouds can form at different altitudes in the atmosphere, depending on the conditions present. Low-level nimbus clouds, such as nimbostratus clouds, typically form below 6,500 feet and are associated with steady, light to moderate rainfall. Mid-level nimbus clouds, such as altostratus clouds, form between 6,500 and 20,000 feet and can bring light rain or snow. High-level nimbus clouds, such as cirrostratus clouds, form above 20,000 feet and are associated with thin, wispy clouds that can produce light precipitation.

In conclusion, a characteristic of a nimbus cloud is its ability to produce precipitation, making it an important indicator of impending weather conditions. Whether it's a gentle rain shower from a nimbostratus cloud or a powerful thunderstorm from a cumulonimbus cloud, these clouds play a crucial role in the water cycle and the Earth's climate system.

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